endstream /Count 5 Aftershock sequence of the 1994, Mw 6.8, Liwa Earthquake (Indonesia): Seismic Rupture process in a volcanic arc /Metadata 4 0 R We discuss the results in the light of historical seismicity, surface observations before and after the Liwa earthquake [Bellier and Sdbrier, 1994; Duquesnoy et … You can help Wikipedia by expanding it. /Type /Catalog Deformation related to the 1994 Liwa Earthquake derived from geodetic measurements. /Parent 2 0 R 1994. >> We present the aftershock activity following the February 15, 1994, Mw 6.8 earthquake which was strongly felt in southern Sumatra, Indonesia, near the Great Sumatran Fault (GSF). A narrow seismic gap underlines the active volcanic area of Suwoh. Both earthquakes occurred inland of Sumatra and were caused by the activity of the Sumatra fault. /Contents [15 0 R 16 0 R 17 0 R 18 0 R 19 0 R 20 0 R 21 0 R 22 0 R] 1994年北岭地震（英語： 1994 Northridge earthquake ）是發生在美国 加州 洛杉矶北岭区的地震，发生于1994年1月17日（UTC-8）。 xڝYɎ���+��H��2 ��wYtu�z�wd�ߏ8I�۷����MQIe�k����R`)���-/_��_���������~�q 1������JZ.��5�����͹��9s.��%���D�����;��3�gtΕ�\��s�Q������K�����������e]�krA����ƿ�Dx���?���:V��KO�K��:��oB�����6��������J��B������_���'�d���E�[#$�H� ��n|�Ze�G? 11 0 obj endobj /ModDate (D:20160205211242-05'00') The deformation field around the southern Great Sumatran Fault (GSF) in the vicinity of the February 15 1994 Mw=6.8 Liwa earthquake has been determined by geodetic survey. /Creator ��w�r���Ο��sտb唛L���bB�c���b|\N����E�> � 5;�b��U CCGd���5l�iYP endobj endobj endobj During the experiment, the NW segment (from Suwoh up to 15 km SE of the Ranau lake caldera, an old right-stepover pull-apart) was very active. /Type /Page %���� The earthquake had an initial Richter reading of 6.5, according to officials in Jakarta. 1990s portal. /Kids [3 0 R 6 0 R 7 0 R 8 0 R 9 0 R] Notice, Smithsonian Terms of endobj We present the aftershock activity following the February 15, 1994, Mw 6.8 earthquake which was strongly felt in southern Sumatra, Indonesia, near the Great Sumatran Fault (GSF). /WPS-JOURNALDOI (10.1002/\(ISSN\)1944-8007) >> /MediaBox [0.0 0.0 582.0 813.0] Earthquakes in the year 1994 . /Pages 2 0 R /Rotate 0 Earth sciences portal. /CropBox [0.0 0.0 582.0 813.0] 4 0 obj >> Geodetic trilateration and Global Positioning System (GPS) measurements were carried out in July 1991 in the Ranau Lake-Liwa area. Use, Smithsonian /Type /Page 6 0 obj Aftershocks mostly locate in a broad zone of 55 × 20 km² near two active NW-trending strike-slip segments of the GSF separated by a recent caldera, Suwoh. 10 0 obj The southern GSF horizontally displaced recent geomorphic features and has been reactivated by earthquakes with consistent lateral displacement (the M w =6.8 Liwa 1994 earthquake is characterised by a co-seismic deformation related with a GSF right-lateral displacement of about 70 cm, Duquesnoy et al., 1996), showing that even for a low obliquity, slip-partitioning exists. 1992年弗洛雷斯地震 （ 英语 ： 1992 Flores earthquake ） 1994年利哇地震 （ 英语 ： 1994 Liwa earthquake ） 1994年爪哇地震; 1996年比亚克地震 （ 英语 ： 1996 Biak earthquake ） 2000年恩加诺地震 （ 英语 ： 2000 Enggano earthquake ） Agreement NNX16AC86A, Is ADS down? /Type /Page www.PrincetonImaging.com WikiZero Özgür Ansiklopedi - Wikipedia Okumanın En Kolay Yolu . >> Great Sumatran Fault This tectonics article is a stub. /MediaBox [0.0 0.0 595.28 841.89] Damage caused by tsunami (Indonesia) (a) 1994 Liwa Earthquake (b) 2006 Central Java Earthquake Figure 3. /CropBox [0.0 0.0 582.0 809.0] Wikimedia Commons has media related to Earthquakes of 1994. Category:1994 earthquakes. International audienceWe present the aftershock activity following the February 15, 1994, Mw 6.8 earthquake which was strongly felt in southern Sumatra, Indonesia, near the Great Sumatran Fault (GSF). << Seismology: Seismicity and seismotectonics; Seismology: Earthquake dynamics and mechanics; Tectonophysics: Continental tectonics-general (0905). The ADS is operated by the Smithsonian Astrophysical Observatory under NASA Cooperative Jump to navigation Jump to search. 1994年爪哇地震是指1994年6月3日發生於印度尼西亞爪哇島南部近海的強烈地震。該次地震震央位於南緯10.477度，東經112.835度，震級為mw 7.8級，震源深度約為18.4公里，最大烈度為6 度[1][3]。該次地震引發了一場最高高度為13.9米的巨大海嘯，共造成238人遇難和423人受傷[5]。 No significant instrumental microseismicity has ever been recorded there. escape 1.1 << The region has been frequently affected by earthquake and tsunami, which killed approximately 22,000 people during the 20th century [ADRC, 2000]. /Author UV radiation (sunlight) matters a lot (high UV is good), relative humidity and temperature matter less, but for both, high values are good. At this place, the slip rate is supposed to be low; neverthless, three M>6 events occurred along this segment during this century. stream وقع في جنوب سومطرة إندونيسيا.تم تحديد حجم الزلزال عند 6.9 ميغاواط أو 7.0 ميغاواط أو 7.2 Ms، وفقًا لمصادر مختلفة.. تسبب الزلزال في 207 قتلى و2.000 مصاب. /MediaBox [0.0 0.0 582.0 813.0] 2007-05-03T13:14:52Z At this place, the slip rate is supposed to be low; neverthless, three M>6 events occurred along this segment during this century. << << >> /Im0 33 0 R /Rotate 0 /Contents [27 0 R 28 0 R] /Filter /FlateDecode 1994 Liwa earthquake: 7.0 M w event caused 207 deaths near the southern tip of Sumatra. Search for more papers by this author. We present the aftershock activity following the February 15, 1994, Mw 6.8 earthquake which was strongly felt in southern Sumatra, Indonesia, near the Great Sumatran Fault (GSF). /Resources 10 0 R /Rotate 0 /MediaBox [0.0 0.0 582.0 809.0] /Resources 26 0 R >> /Producer Institut Géographique National, Saint‐Mandé, France. >> uuid:fabf2e93-d373-436b-ac72-abb14ca9954c 1994年爪哇地震是指1994年6月3日发生于印度尼西亚 爪哇岛南部近海的强烈地震。 该次地震震中位于南纬10.477度，东经112.835度，震级为 m w 7.8级，震源深度约为18.4千米，最大烈度为6(vi)度 。 该次地震引发了一场最高高度为13.9米的巨大海啸，共造成238人遇难和423人受伤 。 The deformation field around the southern GSF in the vicinity of the February 15, 1994 Liwa earthquake, which has been determined by geodetic survey (Duquesnoy et al., 1996), confirms this behaviour. /Type /Page Last edited on 27 January 2021, at 06:33. Two weeks after the 1933 Liwa earthquake, a phreatic eruption from Suoh covered the nearby valley floor with ejecta and killed numerous inhabitants (Stehn 1934). /XObject << << application/pdf We use data from both the regional Indonesian network and a local seismic array operating 11 days after the mainshock during one month. >> /Version /1.5 /Rotate 0 /Parent 2 0 R Astrophysical Observatory. ���@�^��I]0c���F!o(P��7r�CiPEx�C8� �Y%�(����8��n��4x'�Bѕ�c�^T۱±�O�^C��N�2���� �F�l��(v�+�K>��C�Bru���j8kD6��`ޢߡ9�,48�!�:�WC)�C��ɵmz�Whjz������\����z�7� ��%�{ɟ7a��61���j����(@���D����>��;Pl��ǐu����U�ת���W���Ù��b���C� ������o�)0��� Hi�H�G�|,M�6��FƨGT�����R��ٷ#R���#� ��Bɻ�(��9����b���v���\=v�׻�Y>ޮ5��� F߳��_������m����@�C��� /MediaBox [0.0 0.0 582.0 812.0] /Length 4303 Read "Aftershock sequence of the 1994, Mw 6.8, Liwa Earthquake (Indonesia): Seismic Rupture process in a volcanic arc, Geophysical Research Letters" on DeepDyve, the largest online rental service for scholarly research with thousands of academic publications available at your fingertips. Two weeks after the 1933 Liwa earthquake, a phreatic eruption from Suoh covered the nearby val-ley floor with ejecta and killed numerous inhabitants (tehn 1934)ollowing the 1994 Liwa earthquake, which appears to have been limited in rupture extent by the Suoh stepover, there was sudden increase in geothermal We conclude that the rupture process along the GSF is controlled both by volcanism and structures, and that the volcanic activity affects the mechanical properties of the crust only in a narrow zone. The activity of Sunda subduction zone in the recent years caused the 2000 Bengkulu 2 0 obj We have imaged rock density distribution beneath Liwa fracture zone in the southern part of the the Sumatran Fault Zone by modelling and inverting Bouguer gravity data in two-and three-dimensional environments, respectively. Abstract. /WPS-PROCLEVEL (2) /CropBox [0.0 0.0 582.0 813.0] /Type /Metadata Among the destructive earthquakes were the 1976 Jayapura (6,000 killed), 1994 Liwa (210 killed), and the 2000 Bengkulu (90 killed) i�-w~LL���RI��E#��#K;��(� � �ŀxC�]2r�F��ԍ ��)-nL��(6�q /Annots [12 0 R 13 0 R] %PDF-1.4 O. Bellier. 1989. History portal. << The 1994 Liwa earthquake occurred on February 16 at 00:07 local time. Christina Widiwijayanti, Jacques Déverchère, Rémy Louat, Michel Sébrier, Hery Harjono, Michel Diament, Dannie Hidayat << This earthquake was felt as far away as Makassar, the capital of South Sulawesi, and Palu in Central Sulawesi.Several buildings were reportedly destroyed in neighboring cities, including a … endobj /Parent 2 0 R endobj << /Subject /Parent 2 0 R >> /ProcSet [/PDF /Text /ImageC /ImageB /ImageI] /Type /Page URA‐CNRS 1369, Orsay, France. endobj Seismology: Seismicity and seismotectonics; Seismology: Earthquake dynamics and mechanics; Tectonophysics: Continental tectonics—general; Volcanology: General or miscellaneous The magnitude of the earthquake was put at M w 6.9, M w 7.0, or M s 7.2, according to different sources. On January 1, 1996, at 4:05 p.m. Central Indonesia Time, a powerful earthquake with an epicenter in the Makassar Strait struck north of Minahasa on the island of Sulawesi, Indonesia. 8 0 obj /Keywords (http://dx.doi.org/10.1029/96GL02048, doi:10.1029/96GL02048) << /Subtype /XML Earthquakes in Indonesia since 1950 The strongest earthquake in Indonesia happened on 12/26/2004 in the region Sumatra (Aceh: Off West Coast) with a magnitude of 9.1 on the Richter scale. 3 0 obj /Type /Pages stream Pacific Ring of Fire; References External links. 2012-07-18T14:14:41-04:00 As first suggested by the aftershock distribution and the lack of coseismic rupture at the surface, the 20 focal mechanisms determined provide evidence for various post-seismic stress adjustments on secondary faults located in the Ranau-Suwoh paleo-pull-apart graben. From Wikipedia, the free encyclopedia. >> 1 0 obj /Contents [30 0 R 31 0 R] The Indonesian region is prone to earthquake and tsunami disasters. /Contents [24 0 R 25 0 R] /Title زلزال ليوا وقع يوم 16 فبراير 1994م الساعة 00:07 بالتوقيت المحلي. Weather Charts: New Covid-19 forecasts: Per the US DHS, the half-life of the SARS-CoV-2 virus in open air is inversely correlated to UV radiation, relative humidity, and temperature.Choose those graphs below for a rough estimate. /Rotate 0 The earthquake registered a magnitude 7.9 on the moment magnitude scale and was centered off Tolitoli Regency in Cent 7 0 obj The shifting of tectonic plates in a depth of 53 km resulted in 1001 deaths. We present here the aftershock distribution, fault plane solutions, and the deduced stress field. Out-of-plane failure of brick masonry wall (Indonesia) >> << At this place, the slip rate is supposed to be low; neverthless, three M>6 events occurred along this segment during this century. << The United States Geological Survey in Washington put the magnitude at … Less than 20% of the aftershocks are directly linked to the main rupture, a nearly pure right-lateral strike-slip faulting reaching 25 km depth. /Length 1795 No significant instrumental microseismicity has ever been recorded there. Th. /WPS-ARTICLEDOI (10.1029/96GL02048) /CreationDate (D:20210303173433-00'00') /CropBox [0.0 0.0 595.28 841.89] Liwa earthquake of February 16th, 1994 (6.5 Mb) was located in Sumatera fault zone shown the right-lateral strike-slip fault focal mechanism, where the west block of Liwa City region relatively moved to the north and east block to the South. /Font 32 0 R endobj June 24, 1933: M w 7.6 event; See also. 2012-07-18T14:14:41-04:00 /CropBox [0.0 0.0 582.0 812.0] It was located in southern Sumatra, Indonesia. /Im1 34 0 R http://dx.doi.org/10.1029/96GL02048, doi:10.1029/96GL02048 /OpenAction [3 0 R /Fit] >> /Resources 14 0 R The 1994 Aftershocks mostlylocatein a broadzoneof 55x20km2near Liwa earthquake was thus the first opportunity since the two active NW-trending strike-slipsegmentsof the GSF sepa- developmentof temporal and permanentnetworksto study the rated by a recent caldera, Suwoh. /Contents [11 0 R] An earthquake struck the Majene Regency, in the province of West Sulawesi, on the Indonesian island of Sulawesi on 15 January 2021, at 02:28 WITA (18:28 UTC), with a moment magnitude of 6.2. Among them are the 1994 Liwa earthquake (Ms = 7.2) that killed about 210 people, and the 1995 Kerinci earthquake (Ms = 7.0) that killed about 80 people. 5 0 obj /Parent 2 0 R (or is it just me...), Smithsonian Privacy At this place, the slip rate is supposed to be low; neverthless, three M>6 events … /Resources 29 0 R Duquesnoy. (a) 1992 Flores Earthquake (b) 2004 Ache Earthquake Figure 2. 9 0 obj ?�$�u�Q�+�B٘S��[�!v:1X��]�}X���� /Resources 23 0 R endobj uuid:29842e27-574d-4a3e-a199-29b18c922044 �K��D4t'sh�ʂ2���Te�� k�o���d�E�i�͢ck�-�g�be��w��d'��`�)�0)�P8�뇭ݻ� �Y^&1�*k�JMb����З�M��cUs��M %W���Sm��ZL?z�, Seismology: Seismicity and seismotectonics; Seismology: Earthquake dynamics and mechanics; Tectonophysics: Continental tectonics—general; Volcanology: General or miscellaneous, Aftershock sequence of the 1994, Mw 6.8, Liwa Earthquake (Indonesia): Seismic Rupture process in a volcanic arc, Christina Widiwijayanti, Jacques Déverchère, Rémy Louat, Michel Sébrier, Hery Harjono, Michel Diament, Dannie Hidayat.
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